Articles | Volume 22, issue 4
https://doi.org/10.5194/acp-22-2569-2022
https://doi.org/10.5194/acp-22-2569-2022
Research article
 | 
25 Feb 2022
Research article |  | 25 Feb 2022

Long-term fluxes of carbonyl sulfide and their seasonality and interannual variability in a boreal forest

Timo Vesala, Kukka-Maaria Kohonen, Linda M. J. Kooijmans, Arnaud P. Praplan, Lenka Foltýnová, Pasi Kolari, Markku Kulmala, Jaana Bäck, David Nelson, Dan Yakir, Mark Zahniser, and Ivan Mammarella

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on acp-2021-721', Jürgen Kesselmeier, 03 Sep 2021
  • RC2: 'Comment on acp-2021-721', M.E. Whelan, 09 Sep 2021
  • RC3: 'Comment on acp-2021-721', Anonymous Referee #3, 10 Sep 2021
  • AC1: 'Comment on acp-2021-721', Kukka-Maaria Kohonen, 24 Nov 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Kukka-Maaria Kohonen on behalf of the Authors (24 Nov 2021)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (29 Nov 2021) by Marc von Hobe
RR by Jürgen Kesselmeier (09 Dec 2021)
RR by Anonymous Referee #3 (14 Dec 2021)
RR by M.E. Whelan (19 Jan 2022)
ED: Publish subject to minor revisions (review by editor) (20 Jan 2022) by Marc von Hobe
AR by Kukka-Maaria Kohonen on behalf of the Authors (21 Jan 2022)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (21 Jan 2022) by Marc von Hobe
AR by Kukka-Maaria Kohonen on behalf of the Authors (26 Jan 2022)  Manuscript 
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Short summary
Carbonyl sulfide (COS) provides new insights into carbon cycle research. We present an easy-to-use flux parameterization and the longest existing time series of forest–atmosphere COS exchange measurements, which allow us to study both seasonal and interannual variability. We observed only uptake of COS by the forest on an annual basis, with 37 % variability between years. Upscaling the boreal COS uptake using a biosphere model indicates a significant missing COS sink at high latitudes.
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